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Observations of Recent Arctic Sea Ice Volume Loss and Its Impact on Ocean-Atmosphere Energy Exchange and Ice Production

机译:近期北极海冰量损失及其对海洋-大气能量交换和制冰的影响的观测

摘要

Using recently developed techniques we estimate snow and sea ice thickness distributions for the Arctic basin through the combination of freeboard data from the Ice, Cloud, and land Elevation Satellite (ICESat) and a snow depth model. These data are used with meteorological data and a thermodynamic sea ice model to calculate ocean-atmosphere heat exchange and ice volume production during the 2003-2008 fall and winter seasons. The calculated heat fluxes and ice growth rates are in agreement with previous observations over multiyear ice. In this study, we calculate heat fluxes and ice growth rates for the full distribution of ice thicknesses covering the Arctic basin and determine the impact of ice thickness change on the calculated values. Thinning of the sea ice is observed which greatly increases the 2005-2007 fall period ocean-atmosphere heat fluxes compared to those observed in 2003. Although there was also a decline in sea ice thickness for the winter periods, the winter time heat flux was found to be less impacted by the observed changes in ice thickness. A large increase in the net Arctic ocean-atmosphere heat output is also observed in the fall periods due to changes in the areal coverage of sea ice. The anomalously low sea ice coverage in 2007 led to a net ocean-atmosphere heat output approximately 3 times greater than was observed in previous years and suggests that sea ice losses are now playing a role in increasing surface air temperatures in the Arctic.
机译:通过使用最新开发的技术,我们结合了来自冰,云和陆地高程卫星(ICESat)的干舷数据以及雪深模型,估算了北极盆地的雪和海冰厚度分布。这些数据与气象数据和热力学海冰模型一起使用,可以计算2003-2008年秋冬季期间的海洋-大气热交换和冰量产生。计算得出的热通量和冰的增长率与多年冰期的先前观测结果一致。在这项研究中,我们计算了覆盖北极盆地的冰厚度的全部分布的热通量和冰的生长速率,并确定了冰厚度变化对计算值的影响。与2003年相比,观察到海冰变薄,这大大增加了2005-2007年秋季海洋和海洋的热通量。尽管冬季海冰厚度也有所减少,但发现冬季热通量受观察到的冰厚变化影响较小。由于海冰面积的变化,在秋季,北极海洋和海洋的净热量输出也大大增加。 2007年异常低的海冰覆盖面积导致海洋大气净热量输出比前几年高出约3倍,这表明海冰损失现在正在增加北极的地表气温。

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